Mass transfers during fluid-rock interactions at divergent and convergent plate boundaries
Date Issued
2019-02-04
Author(s)
Supervisors
Referees
Abstract
Fluids and reactions between fluids and rock evoke significant mass and energy transfers in the marine realm. Phyllosilicate-rich shear zone rocks from a detachment fault zone (Mid-Atlantic Ridge) formed by hydrothermal alteration of hybrid ultramafica mafic rocks. Extensional strain and deformation focus in these weak lithologies and initiate a feedback loop between hydration and strain localization, which likely play a key role in detachment faults worldwide. Carbonates, precipitated from CO2-rich, oxidizing fluids, have formed in veins in metavolcanic and -sedimentary clasts at depths <20 km within the subduction channel (Mariana subduction system). Their existence proofs of C mobilization from the slab at shallow portions of subduction zones. Serpentinites from the basal plane of the mantle wedge (Mariana subduction zone) contain high contents of fluid-mobile elements (Li, B, Sr, Rb, Cs, Ba) that were mobilized during dehydration of the slab. Element concentrations vary with slab-depths and the sources of the serpentinization fluids, and provide a continuous record of slab dehydration reactions.
Subjects
Geosciences
;
Metamorphic geology
;
Fluid-rock interactions
;
Mid-ocean ridges
;
Subduction zones
Institution
Type
Dissertation
Secondary publication
No
Language
English
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00107083-1.pdf
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25.97 MB
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Adobe PDF
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